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Boroo

Selenge, North Khentii Gold Belt (Dzuunmod area), Mongolia

Orogenic goldAu

Type
Orogenic gold (veins, disseminations and stockworks)

North Khentii Gold Belt (Khentii basin, Mongol-Okhotsk orogenic belt), Haraa terrane: Haraa Group metasediments (Middle Cambrian to Early Ordovician) cut by the Boroogol granitoid complex (Ordovician) and the Dzuunmod rhyolitic subvolcanic complex; sericitic, siliceous and potassic alteration, pyrite and arsenopyrite with invisible gold, late native gold. Fluid calculated at 275 °C (arsenopyrite geothermometer) at δ18O +6.3 to +9.3 ‰, of metamorphic origin; heterogeneous sulphur source, wall-rock sulphidation according to Kim et al. (2020). Largest deposit of the district, open-pit mined from 2004 to 2010 (over 50 t gold), controlled by the Boroo thrust (Yeroogol system) between the Haraa Group and the Boroogol complex; mineralisation ages of 208.3 ± 1.9 to 186.2 ± 1.6 Ma (Cluer et al., 2005). Coordinates not given.

δ34S in ‰ (per mil) Values of the same system

Standard : V-CDT

ValueRangenMineral or matrixSource
1.85 ± 3.32 ‰−0.5 / 4.2 ‰2pyrite of sulphidised sandstone and granite (BR-P-6, MDD-008)
Mean and standard deviation recalculated from 2 analyses.
Kim et al. (2020), Geology, mineralogy and stable isotope geochemistry of the Dzuunmod ar…

δ18O in ‰ (per mil) Values of the same system

Standard : V-SMOW

ValueRangenMineral or matrixSource
16.2 ‰16.2 / 16.2 ‰2vein quartz (BDD-105, KH-BOR-4)
Mean and standard deviation recalculated from 2 analyses, fluid calculated at 275 °C (Friedman and O'Neil, 1977) of +7.9 ‰.
Kim et al. (2020), Geology, mineralogy and stable isotope geochemistry of the Dzuunmod ar…

Deposits of the same type

Cite this page

IsoFind Atlas (2026). Boroo, isotope signatures. https://www.isofind.tech/isotopes/en/deposits/boroo/ (accessed 2026-10-14).

@misc{isofind2026borooisotopesignatures,
  title = {Boroo, isotope signatures},
  author = {{IsoFind Atlas}},
  year = {2026},
  url = {https://www.isofind.tech/isotopes/en/deposits/boroo/},
  note = {Accessed 2026-10-14}
}

Updated : 2026-10-14